
Infectious Diseases and Climate Influences
Source: OET Version 1/0
مدت زمان تمرین این بخش: 45 دقیقه
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Complex dynamic relationships between humans, pathogens, and the environment lead to the emergence of new diseases and the re-emergence of old ones. Due to concern about the impact of increasing global climate variability and change, many recent studies have focused on relationships between infectious disease and climate.
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Complex relationships between humans, pathogens, and the environment cause new diseases to appear and old ones to come back. Because of worries about changing global climate, many recent studies have looked at how infectious diseases are related to climate.
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Climate can be an important determinant of vector-borne disease epidemics: geographic and seasonal patterns of infectious disease incidence are often, though not always, driven by climate factors. Mosquito- borne diseases, such as malaria, dengue fever, and Ross River virus, typically show strong seasonal and geographic patterns, as do some intestine diseases. These patterns are unsurprising, given the influence of climate on pathogen replication, vector and disease reservoir populations, and human societies. In Sweden, a trend toward milder winters and early spring arrival may be implicated in an increased incidence of tick-borne encephalitis. The recent resurgence of malaria in the East African highlands may be explained by increasing temperatures in that region. However, as yet there are relatively few studies showing clear climatic influences on infectious diseases at interannual or longer timescales.
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Climate can greatly affect the spread of vector-borne diseases. The geographic and seasonal patterns of these diseases are often influenced by climate, though not always. Diseases spread by mosquitoes, such as malaria, dengue fever, and Ross River virus, typically follow strong seasonal and geographic trends, as do some intestinal diseases. This is because climate affects how pathogens grow, the populations of vectors and disease reservoirs, and human activities. In Sweden, milder winters and earlier springs might be causing more cases of tick-borne encephalitis. The recent increase in malaria cases in the East African highlands might be due to rising temperatures. However, there are still few studies showing clear links between climate and infectious diseases over long periods.
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The semi-regular El Niño climate cycle, centred on the Pacific Ocean, has an important influence on interannual climate patterns in many parts of the world. This makes El Niño an attractive, albeit imperfect, analogue for the effects of global climate change. In Peru, daily admissions for diarrhoea increased by more than 2-fold during an El Niño event, compared with expected trends based on the previous five years. There is evidence of a relationship between El Niño and the timing of cholera epidemics in Peru and Bangladesh; of ciguatera in the Pacific islands; of Ross River virus epidemics in Australia; and of dengue and malaria epidemics in several countries. The onset of meningococcal meningitis in Mali is associated with large-scale atmospheric circulation.
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The El Niño climate cycle, centered on the Pacific Ocean, significantly influences yearly climate patterns worldwide. This makes El Niño a useful, though imperfect, model for studying global climate change effects. In Peru, daily hospital admissions for diarrhea more than doubled during an El Niño event compared to the previous five years. There is evidence linking El Niño to the timing of cholera outbreaks in Peru and Bangladesh, ciguatera in the Pacific islands, Ross River virus in Australia, and dengue and malaria epidemics in several countries. The start of meningococcal meningitis in Mali is linked to large-scale atmospheric changes.
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These studies were performed mostly at country scale, reflecting the availability of data sources and, perhaps, the geographically local effects of El Niño on climate. In part because of this geographic “patchiness” of the epidemiological evidence, the identification of climatic factors in infectious disease dynamics, and the relative importance of the different factors, remains controversial. For example, it has been suggested that climate trends are unlikely to contribute to the timing of dengue epidemics in Thailand. However, recent work has shown a strong but transient association between dengue incidence and El Niño in Thailand. This association may possibly be caused by a “pacemaker-like” effect in which intrinsic disease dynamics interact with climate variations driven by El Niño to propagate travelling waves of infection.
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These studies were mainly done at the country level, reflecting the available data and the local effects of El Niño on climate. Because of this geographic “patchiness” in the evidence, identifying the role of climate in infectious disease spread and the importance of different factors remains debated. For example, some suggest that climate trends don’t affect the timing of dengue outbreaks in Thailand. However, recent research has found a strong but short-lived link between dengue cases and El Niño in Thailand. This may be due to a “pacemaker-like” effect where disease dynamics interact with El Niño-driven climate variations to spread waves of infection.
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A new study on cutaneous leishmaniasis by Chaves and Pascual also provides fresh evidence of a relationship between climate and vector-borne disease. Chaves and Pascual use a range of mathematical tools to illustrate a clear relationship between climatic variables and the dynamics of cutaneous leishmaniasis, a skin infection transmitted by sandflies. In Costa Rica, cutaneous leishmaniasis displays three-year cycles that coincide with those of El Niño. Chaves and Pascual use this newly demonstrated association to enhance the forecasting ability of their models and to predict the epidemics of leishmaniasis up to one year ahead. Interestingly, El Niño was a better predictor of disease than temperature, possibly because this large-scale index integrates numerous environmental processes and so is a more biologically relevant measure than local temperature. As the authors note, the link between El Niño and epidemics of leishmaniasis might be explained by large-scale climate effects on population susceptibility. Susceptibility, in turn, may be related to lack of specific immunity or poor nutritional status, both of which are plausibly influenced by climate.
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A new study by Chaves and Pascual on cutaneous leishmaniasis shows a link between climate and vector-borne disease. They use mathematical tools to show how climate variables affect the dynamics of cutaneous leishmaniasis, a skin infection spread by sandflies. In Costa Rica, cutaneous leishmaniasis follows three-year cycles that match those of El Niño. Chaves and Pascual use this connection to improve their models’ ability to forecast leishmaniasis epidemics up to a year in advance. Interestingly, El Niño was a better disease predictor than temperature, likely because it reflects many environmental processes and is more relevant biologically than local temperature. The authors suggest that El Niño’s link to leishmaniasis epidemics might be due to its large-scale climate effects on people’s susceptibility, which could be related to lack of immunity or poor nutrition, both influenced by climate.
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Chaves and Pascual have identified a robust relationship between climate and disease, with changes over time in average incidence and in cyclic components. The dynamics of cutaneous leishmaniasis evolve coherently with climatic variables including temperature and El Niño indices, demonstrating a strong association between these variables, particularly after 1996. Long-term changes in climate, human demography, and social features of human populations have large effects on the dynamics of epidemics as underlined by the analyses of some large datasets on whooping cough and measles. Another illuminating example is the transient relationship between cholera prevalence and El Niño oscillations. In Bangladesh, early in the 20th century, cholera and El Niño appeared unrelated, yet a strong association emerged in 1980–2001. Transient relationships between climate and infectious disease may be caused by interactions between climate and intrinsic disease mechanisms such as temporary immunity. If population susceptibility is low, even large increases in transmission potential due to climate forcing will not result in a large epidemic.
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Chaves and Pascual have found a strong link between climate and disease, showing changes in average incidence and cyclic patterns over time. The dynamics of cutaneous leishmaniasis align well with climatic variables like temperature and El Niño indices, especially after 1996. Long-term changes in climate, human population growth, and social factors significantly affect epidemic dynamics, as shown in large datasets on whooping cough and measles. Another example is the changing relationship between cholera and El Niño. In Bangladesh, cholera and El Niño were unrelated early in the 20th century, but a strong link appeared from 1980 to 2001. These transient relationships may be due to interactions between climate and disease mechanisms like temporary immunity. If the population’s susceptibility is low, even significant increases in disease transmission due to climate changes won’t lead to a large epidemic.
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A deeper understanding of infectious disease dynamics is important in order to forecast, and perhaps forestall, the effects of dramatic global social and environmental changes. Conventional statistical methods may fail to reveal a relationship between climate and health when discontinuous associations are present. Because classical methods quantify average associations over the entire dataset, they may not be adequate to decipher long-term but discontinuous relationships between environmental exposures and human health. On the other hand, relationships between climate and disease could signal problems for disease prediction. Unless all important effects are accounted for, dynamic forecast models may prove to have a limited shelf life.
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Understanding infectious disease dynamics is crucial for predicting and possibly preventing the impacts of significant global social and environmental changes. Traditional statistical methods might miss the link between climate and health if the associations are not continuous. These classical methods measure average associations over the entire dataset and may not capture long-term but irregular relationships between the environment and health. On the other hand, climate-disease links could complicate disease prediction. If all significant factors aren’t considered, dynamic forecast models might not remain accurate for long.